Petrography of alluvial sands as a past and present environmental indicator： Case of the Loire River （France）
Four sample sets of the Upper and Middle Loire river sands were analyzed in order to study the impact of natural and anthropogenic factors on their petrographic composition in space （on an 800 km stretch） and time.Composition was determined by modal analysis of three sand-size fractions using a pola...
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| Published in | 国际泥沙研究：英文版 Vol. 28; no. 3; pp. 285 - 303 |
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| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
2013
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| Subjects | |
| Online Access | Get full text |
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| Summary: | Four sample sets of the Upper and Middle Loire river sands were analyzed in order to study the impact of natural and anthropogenic factors on their petrographic composition in space （on an 800 km stretch） and time.Composition was determined by modal analysis of three sand-size fractions using a polarizing optical microscope and calculated for each sample （＂standard sand＂ =Sst）.The watershed is composed mainly of endogenic （Massif Central） and sedimentary （southern Parisian Basin） rocks.B-set sands collected in channels for different water flows in 1996show that Sst compositions vary by only 5 ％.Present-day sands in the Upper Loire and Middle Loire have very high petrographic immaturity comparing to others worldwide fluvial sands,although bio-climatic conditions favor sand maturation by source-rock weathering in the watershed.This shows the strong impact of the Massif Central on sediment yield due to relief rejuvenation as a consequence of the formation of the Alps during the Quaternary.Fluvial sands stored during the Weichselian and the Holocene in the Middle Loire floodplain,although partly weathered since their deposition,show higher inputs from the endogenic rocks of the Massif Central than present-day deposits.This can be explained by Weichselian periglacial conditions and the development of crop farming since the Neolithic,which favored mechanical erosion,particularly in the Massif Central which is characterized by a cold,humid climate and steep slopes.The upstream-downstream change in the composition of presently deposited sand is low in the diked area.It shows however that basalt and some heavy mineral grains are vulnerable to abrasion during transport and indicates a marked sediment yield from ancient sediment stored in the floodplain.This is in line with the high incision of the river bed over the last 150 years partly due to dam construction and aggregate mining. |
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| Bibliography: | 11-2699/P Fluvial sand; Sand petrography; Sediment source; Tectonics impact; Human impact; Loire river Four sample sets of the Upper and Middle Loire river sands were analyzed in order to study the impact of natural and anthropogenic factors on their petrographic composition in space （on an 800 km stretch） and time.Composition was determined by modal analysis of three sand-size fractions using a polarizing optical microscope and calculated for each sample （＂standard sand＂ =Sst）.The watershed is composed mainly of endogenic （Massif Central） and sedimentary （southern Parisian Basin） rocks.B-set sands collected in channels for different water flows in 1996show that Sst compositions vary by only 5 ％.Present-day sands in the Upper Loire and Middle Loire have very high petrographic immaturity comparing to others worldwide fluvial sands,although bio-climatic conditions favor sand maturation by source-rock weathering in the watershed.This shows the strong impact of the Massif Central on sediment yield due to relief rejuvenation as a consequence of the formation of the Alps during the Quaternary.Fluvial sands stored during the Weichselian and the Holocene in the Middle Loire floodplain,although partly weathered since their deposition,show higher inputs from the endogenic rocks of the Massif Central than present-day deposits.This can be explained by Weichselian periglacial conditions and the development of crop farming since the Neolithic,which favored mechanical erosion,particularly in the Massif Central which is characterized by a cold,humid climate and steep slopes.The upstream-downstream change in the composition of presently deposited sand is low in the diked area.It shows however that basalt and some heavy mineral grains are vulnerable to abrasion during transport and indicates a marked sediment yield from ancient sediment stored in the floodplain.This is in line with the high incision of the river bed over the last 150 years partly due to dam construction and aggregate mining. |
| ISSN: | 1001-6279 |